The role of sea-level change and marine anoxia in the Frasnian–Famennian (Late Devonian) mass extinction

2008/03/21 by David P.G. Bond, Paul B. Wignall · 4 citations
Earth and Planetary Sciences · #Geological and Geophysical Studies #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.palaeo.2008.02.015

openalex publication_date 2008/03/21 · crossref created 2008/03/21 · crossref issued 2008/06/01 · crossref published 2008/06/01 · crossref published-print 2008/06/01 · crossref deposited 2020/05/03 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/17 · crossref indexed 2026/08/04

Citations

• Decision on the Devonian-Carboniferous boundary stratotype

Cited by

• Evidence for shallow-water ‘Upper Kellwasser’ anoxia in the Frasnian–Famennian reefs of Alberta, Canada
• Plant fossil record and survival analyses
• A sulfidic driver for the end-Ordovician mass extinction
• Extinction event [wikipedia]